FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2050382092> ?p ?o ?g. }

• W2050382092 endingPage "772" @default.
• W2050382092 startingPage "755" @default.
• W2050382092 abstract "We use new space geodetic data from very long baseline interferometry and satellite laser ranging combined with other geodetic and geologic data to study contemporary deformation in the Basin and Range province of the western United States. Northwest motion of the central Sierra Nevada block relative to stable North America, a measure of integrated Basin and Range deformation, is 12.1±1.2 mm/yr oriented N38°W±5° (one standard error), in agreement with previous geological estimates within uncertainties. This velocity reflects both east‐west extension concentrated in the eastern Basin and Range and north‐northwest directed right lateral shear concentrated in the western Basin and Range. Ely, Nevada is moving west at 4.9±1.3 mm/yr relative to stable North America, consistent with dip‐slip motion on the north striking Wasatch fault and other north striking normal faults. Comparison with ground‐based geodetic data suggests that most of this motion is accommodated within ∼50 km of the Wasatch fault zone. Paleoseismic data for the Wasatch fault zone and slip rates based on seismic energy release in the region both suggest much lower slip rates. The discrepancy may be explained by some combination of additional deformation away from the Wasatch fault itself, aseismic slip, or a seismic rate that is anomalously low with respect to longer time averages. Deformation in the western Basin and Range province is also largely confined to a relatively narrow boundary zone and in our study area is partitioned into the eastern California shear zone, accommodating 10.7±1.6 mm/yr of north‐northwest directed right‐lateral shear, and a small component (∼1 mm/yr) of west‐southwest ‐ east‐northeast extension. A slip rate budget for major strike‐slip faults in our study area based on a combination of local geodetic or late Quaternary geologic data and the regional space geodetic data suggests the following rates of right‐lateral slip: Owens Valley fault zone, 3.9±1.1 mm/yr; Death Valley‐Furnace Creek fault zone, 3.3±2.2 mm/yr; White Mountains fault zone in northern Owens Valley, 3.4±1.2 mm/yr; Fish Lake Valley fault zone, 6.2±2.3 mm/yr. In the last few million years the locus of right‐lateral shear in the region has shifted west and become more north trending as slip on the northwest striking Death Valley‐Furnace Creek fault zone has decreased and is increasingly accommodated on the north‐northwest striking Owens Valley fault zone." @default.
• W2050382092 created "2016-06-24" @default.
• W2050382092 creator A5036916615 @default.
• W2050382092 creator A5068801451 @default.
• W2050382092 creator A5089098731 @default.
• W2050382092 creator A5089288874 @default.
• W2050382092 date "1995-08-01" @default.
• W2050382092 modified "2023-10-11" @default.
• W2050382092 title "Constraints on present‐day Basin and Range deformation from space geodesy" @default.
• W2050382092 cites W1526295891 @default.
• W2050382092 cites W1536573502 @default.
• W2050382092 cites W1551629520 @default.
• W2050382092 cites W1586495112 @default.
• W2050382092 cites W1613146828 @default.
• W2050382092 cites W1964091216 @default.
• W2050382092 cites W1964151654 @default.
• W2050382092 cites W1965565578 @default.
• W2050382092 cites W1968847917 @default.
• W2050382092 cites W1984034703 @default.
• W2050382092 cites W1985251386 @default.
• W2050382092 cites W1988915166 @default.
• W2050382092 cites W1990167266 @default.
• W2050382092 cites W1990579454 @default.
• W2050382092 cites W2003432404 @default.
• W2050382092 cites W2004219107 @default.
• W2050382092 cites W2006915059 @default.
• W2050382092 cites W2011273489 @default.
• W2050382092 cites W2012547949 @default.
• W2050382092 cites W2020626050 @default.
• W2050382092 cites W2022016919 @default.
• W2050382092 cites W2024842100 @default.
• W2050382092 cites W2024953052 @default.
• W2050382092 cites W2041108792 @default.
• W2050382092 cites W2043458211 @default.
• W2050382092 cites W2048362440 @default.
• W2050382092 cites W2052426250 @default.
• W2050382092 cites W2053609724 @default.
• W2050382092 cites W2056418513 @default.
• W2050382092 cites W2066201464 @default.
• W2050382092 cites W2066635404 @default.
• W2050382092 cites W2073798361 @default.
• W2050382092 cites W2074626981 @default.
• W2050382092 cites W2079238116 @default.
• W2050382092 cites W2081547165 @default.
• W2050382092 cites W2085930405 @default.
• W2050382092 cites W2086619209 @default.
• W2050382092 cites W2088711685 @default.
• W2050382092 cites W2089746061 @default.
• W2050382092 cites W2093160875 @default.
• W2050382092 cites W2098328952 @default.
• W2050382092 cites W2111061528 @default.
• W2050382092 cites W2120403466 @default.
• W2050382092 cites W2121775416 @default.
• W2050382092 cites W2124173505 @default.
• W2050382092 cites W2128258588 @default.
• W2050382092 cites W2135494568 @default.
• W2050382092 cites W2137476333 @default.
• W2050382092 cites W2141824013 @default.
• W2050382092 cites W2142536098 @default.
• W2050382092 cites W2144677198 @default.
• W2050382092 cites W2154484095 @default.
• W2050382092 cites W2155500845 @default.
• W2050382092 cites W2159624644 @default.
• W2050382092 cites W2171456380 @default.
• W2050382092 cites W2339461071 @default.
• W2050382092 cites W2380374024 @default.
• W2050382092 cites W2468637599 @default.
• W2050382092 cites W367557070 @default.
• W2050382092 cites W4234066025 @default.
• W2050382092 doi "https://doi.org/10.1029/95tc00931" @default.
• W2050382092 hasPublicationYear "1995" @default.
• W2050382092 type Work @default.
• W2050382092 sameAs 2050382092 @default.
• W2050382092 citedByCount "171" @default.
• W2050382092 countsByYear W20503820922012 @default.
• W2050382092 countsByYear W20503820922013 @default.
• W2050382092 countsByYear W20503820922014 @default.
• W2050382092 countsByYear W20503820922015 @default.
• W2050382092 countsByYear W20503820922016 @default.
• W2050382092 countsByYear W20503820922017 @default.
• W2050382092 countsByYear W20503820922018 @default.
• W2050382092 countsByYear W20503820922019 @default.
• W2050382092 countsByYear W20503820922020 @default.
• W2050382092 countsByYear W20503820922021 @default.
• W2050382092 countsByYear W20503820922022 @default.
• W2050382092 countsByYear W20503820922023 @default.
• W2050382092 crossrefType "journal-article" @default.
• W2050382092 hasAuthorship W2050382092A5036916615 @default.
• W2050382092 hasAuthorship W2050382092A5068801451 @default.
• W2050382092 hasAuthorship W2050382092A5089098731 @default.
• W2050382092 hasAuthorship W2050382092A5089288874 @default.
• W2050382092 hasBestOaLocation W20503820922 @default.
• W2050382092 hasConcept C109007969 @default.
• W2050382092 hasConcept C121332964 @default.
• W2050382092 hasConcept C127313418 @default.
• W2050382092 hasConcept C13280743 @default.
• W2050382092 hasConcept C151730666 @default.
• W2050382092 hasConcept C155627805 @default.

• next